Chapter 12 Soils Overview Soil Regolith Soil components

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Chapter 12 Soils

Chapter 12 Soils

Overview • • • Soil & Regolith Soil components Soil Properties & Chemistry

Overview • • • Soil & Regolith Soil components Soil Properties & Chemistry

 • Soil – infinitely varying mixture of weathered mineral particles, decaying organic matter,

• Soil – infinitely varying mixture of weathered mineral particles, decaying organic matter, living organisms, gases, and liquid solutions • • Part of the outer “skin” of the earth Occupied by plant roots Thickness of soils varies depending on regional characteristics • Thin in the tropics, thicker in mid-latitudes • Generally thicker on flat land than on slopes Regolith – layer of broken and partly decomposed rock particles that covers bedrock

Soil Components • Inorganic materials • • Sand & silt • • • Approximately

Soil Components • Inorganic materials • • Sand & silt • • • Approximately 45% of soil is inorganic Approximately 50% of soil is air (gas) and/or water Inorganic material is mostly minerals from rocks Largest size particles of soil Composes about half the volume of typical soils Clay • • Smallest sized particles of soil Too small to be seen with the naked eye

Soil Texture Triangle Loam – a relatively balanced soil containing roughly equal parts sand,

Soil Texture Triangle Loam – a relatively balanced soil containing roughly equal parts sand, silt, clay; most productive soil type for plants

 • Organic materials – accounts for 5% of soil • Litter – collection

• Organic materials – accounts for 5% of soil • Litter – collection of dead plant material • • Leaves, twigs, stalks, etc. Rate of decomposition varies depending on climate • • Faster in warm, humid regions Slower in cold and/or dry regions

 • Organic Materials cont. • Humus – dark colored, gelatinous, chemically stable fraction

• Organic Materials cont. • Humus – dark colored, gelatinous, chemically stable fraction of organic matter in the soil • • Results from the decomposition of plant material “black gold” for agriculture • • Catalyst for chemical reactions Reservoir for plant nutrients and soil water

Soil Chemistry • Chemical components of soils have a large influence plants productivity, as

Soil Chemistry • Chemical components of soils have a large influence plants productivity, as well as what types of plants can survive in in the soil • p. H of soils has a great influence as to the types of plants and productivity that can be seen in soils • • Generally speaking, plants are most productive in acidic soils Plants can grow in alkaline (salty) soils, but are usually small, grow slower, and not as productive as plants in acidic soils

Are the soils in the picture more likely to be acidic or alkaline?

Are the soils in the picture more likely to be acidic or alkaline?

Are the soils in the picture more likely to be acidic or alkaline?

Are the soils in the picture more likely to be acidic or alkaline?